Deriving inherent optical property for highly turbid productive inland water from MERIS data by semi-analytical model: A case study in Taihu Lake, China

Authors

  • C. Huang Key Laboratory of Virtual Geographic Environment, Nanjing Normal University, Ministry of Education, Nanjing 210046, China
  • X. Chen Key Laboratory of Virtual Geographic Environment, Nanjing Normal University, Ministry of Education, Nanjing 210046, China
  • Y. Li Key Laboratory of Virtual Geographic Environment, Nanjing Normal University, Ministry of Education, Nanjing 210046, China
  • H. Yang Key Laboratory of Virtual Geographic Environment, Nanjing Normal University, Ministry of Education, Nanjing 210046, China
  • D. Sun College of Remote Sensing, Nanjing University of Information Science and Technology, Nanjing 210046, China
  • C. Le College of Marine Science, University of South Florida, Tampa, Florida, USA
  • L. Xu Key Laboratory of Virtual Geographic Environment, Nanjing Normal University, Ministry of Education, Nanjing 210046, China

Keywords:

support vector machine, scattering and absorption coefficients, remote sensing reflectance

Abstract

Remote estimation of inherent optical properties was greatly challenged by significant spatial-temporal variation and the extreme complexity of bio-optical properties in inland turbid water. The multiband quasi-analytical algorithm has advantages over traditional band ratio and semi-analytical algorithm in that it is based on the remote sensing reflectance model derived from radiative transfer equation and does not need the parameterization of absorption coefficients. An improved model, which used, was developed to retrieve inherent optical properties in high turbid inland water. As a first step, the backscattering coefficient at reference wavelength [bbp0)] was retrieved directly by support vector machine optimization algorithm instead of step 2 in the quasi analytical algorithm for the high correlation between bbp0) and remote sensing reflectance at the near-infrared wavelength. The second step, a semi-analytical support vector machine algorithm, was used to retrieve spectral shape of bbp(λ) instead the step 4 in the quasi analytical algorithm. Part of field-measured dataset collected on November 2006, November 2007, November 2008 and April 2009 in Taihu Lake was used to train the support vector machine model, and the other part was used to test this algorithm. Results indicated that the mean square root of percentage between the derived and measured value of bbp(532 nm) was less than 3.73% and root mean square percentage of ap(442 nm) and ap(532 nm) were 15.29% and 30.45%, respectively. Furthermore, the potential application of this algorithm to MERIS data was investigated by the reduced resolution MERIS satellite image. The result shows that satellite-derived data using the support vector machine model is consistent with in situ measured data. This study advances the semi-analytical model and broadens the application of MERIS data in highly turbid inland waters.

References

Arbones, B., F.G. Figueiras, and Zapata, M., 1996. Determination of phytoplankton absorption coefficient in natural seawater samples: evidence of a unique equation to correct the path length amplification on glass-fiber filters. Mar. Ecol. 17, 293–304.

Babin, M., Morel, A., and Fell, F., 2003. Light scattering properties of marine particles in coastal and open ocean waters as related to the particle mass concentration. Limnol.Oceanogr., 48(3), 843–859.

Cleveland, J.S., and Weidemann, A.D., 1993. Quantifying absorption by aquatic particles: A multiple scattering correction for glass-fiber filters. Limnol.Oceanogr. 38, 1321–1327.

Doerffer, R., and Fisher, J., 1994. Concentrations of chlorophyll, suspended matter, and gelbstoff in case II waters derived from satellite coastal zone color scanner data with inverse modeling methods. J. Geophy. Res, 99, 7475–7466.

Doerffer, R., and Schiller, H., 2007. The MERIS case 2 water algorithms. Int. J. Remote Sensing 28(3), 517–535.

Doerffer, R., and Schiller, H., 2008. MERIS Regional Coastal and Lake Case 2 Water Project Atmospheric Correction ATBD. Version 1.0, GKSS Research Centre Geesthacht, Institute for Coastal Research.

Doerffer, R., Sorensen, K., and Aiken, J., 1999. MERIS potential for coastal zone applications. Int. J. Remote Sensing 20(9), 1809–1818.

Doron, M., Babin, M., Mangin, A., and Hembise, O., 2007. Estimation of light penetration, and horizontal and vertical visibility in oceanic and coastal waters from surface reflectance. J. Geophys. Res. 112: C06003, doi:10.1029/2006JC004007.

Gordon, H.R., Brown, O. B., Evans, R. H., Brown, J. W., SMith, R. C., Baker, K. S., and Clark, C. K., 1988. A semi-analytic radiance model of ocean color. J. Geophys. Res. 93, . 10,909-10,924.

Gould, R.W., Arnone, R.A., and Martinolich, P.M., 1999. Spectral dependence of the scattering coefficient in case 1 and case 2 waters. Applied Optics,38(12), 2377–2383.

Gunn, S.R., 1998. Support Vector Machines for Classification and Regression. Technical Report, University of Southampton, UK.

Kishino, M., Tanaka, A., and Ishizaka, J., 2005. Retrieval of Chlorophyll a, suspended solids, and colored dissolved organic matter in Tokyo Bay using ASTER data. Remote Sens. Environ., 99, 66–74.

Kratzer, S., Brockmann, C., and Moore, G., 2007. Using MERIS full resolution data to monitor coastal waters-A case study from Himmerfjärden, a fjord-like bay in the northwestern Baltic Sea. Remote Sens. Environ., doi:10.1016/j.rse.2007.10.006.

Le, C.F., Li, Y. M., Zha, Y., Sun, D., and Yin, B., 2009. Validation of a Quasi-Analytical Algorithm for Highly Turbid Eutrophic Water of Meiliang Bay in Taihu Lake, China. IEEE Transactions on Geoscience and Remote Sensing, 47(8), 2492–2500.

Lee, Z.P., Carder, K. L., Steward, R. G., Peacock, T. G., Davis, C. O., and Patch, J. S., 1998. An empirical algorithm for light absorption by ocean water based on color. J. Geophys. Res. 103, 27967–27978.

Lee, Z.P., Carder, K.L. Mobley, C. D., Steward, R. G., and Patch, J. S., 1999. Hyperspectral remote sensing for shallow waters: 2. Deriving bottom depths and water properties by optimization. Applied Optics 38, 3831–3843.

Lee, Z.P., Carder, K.L., and Armone, R., 2002. Deriving inherent optical properties from water color: A multi-band quasi-analytical algorithm for optically deep waters. Applied Optics 41, 5755–5772.

Lubac, B., and Loisel, H., 2007. Variability and classification of remote sensing reflectance spectra in the eastern English channel and southern north sea. Remote Sens. Environ., doi:10.1016/j.rse.2007.02.012

Maritorena, S., Siegel, D. A., and Peterson, A. R., 2002. Optimization of a semi-analytical ocean color model for global-scale applications. Applied Optics 41, 2705–2714.

Mitchell, B.G., 1990. Algorithms for determining the absorption coefficient for aquatic particles using the quantitative filter technique. Ocean Optics X, SPIE.

Moore, C., Barnard, A., and Hankins, D., 2004. Spectral Absorption and Attenuation Meter (ac-s) User’s Guide. Revision A America: WET Labs Inc, 5–20

Moore, G.F., and Aiken, J., 2000. Case 2 bright pixel atmospheric correction. Algorithm Theoretical Basis Document, ATBD 2.6. MERIS ESL Doc. No:PO-TN-MEL-GS-0005: http://envisat.esa.int/instruments/meris/pdf/atbd_2_06.pdf.

Mueller, J.L., Fargion, G. S., and McClain, C. R. (Eds.), 2003. Ocean Optics Protocols For Satellite Ocean Color Sensor Validation. . Revision 4, Goddard Space Flight Center, Greenbelt, MD, NASA.

Pope, R., and Fry, E., 1997. Absorption spectrum (380–700 nm) of pure waters: II. Integrating cavity measurements. Applied Optics 36, 8710–8723.

Preisendorfer, R.W., 1976. Hydrologic optics vol. 1: Introduction. Springfield, National Technical Information Service. Also available on CD, Office of Naval Research.

Schroeder, T., Fischer, J., Schuule, M., and Fell, F., 2002. Artificial neural network based atmospheric correction algorithm: Application to MERIS data. Proceedings of the International Society for Optical Engineering (SPIE). Hangzhou, China.

Twardowski, M.S., Boss, E., and Macdonald. J.B., 2001. A model for estimating bulk refractive index from the optical backscattering ratio and the implications for understanding particle composition in case I and case II waters. J. Geophys. Res. 14, 129–142

Ulloa, O., Sathyendranath, S., and Platt T., 1994. Effect of the particle-size distribution on the backscattering ratio in seawater. Applied Optics 33(30), 7070–7077

Wang, M., Son, S., and Harding, L. W., Jr., 2009. Retrieval of diffuse attenuation coefficient in the Chesapeake Bay and turbid ocean regions for satellite ocean color applications. J. Geophys. Res., 114: C10011, doi:10.1029/2009JC005286.

Yan, G.H., and Zhu Y.S., 2009. Parameters Selection Method for Support Vector Machine Regression. Computer Engineering 35(13), 218–220.

Zhang, Y.L., Liu, M. L., Qin, B., van der Woerd, H. J., and Li, J., 2009. Modeling Remote-Sensing Reflectance and Retrieving Chlorophyll-a Concentration in Extremely Turbid Case-2 Waters (Lake Taihu, China). IEEE Transactions on Geoscience and Remote Sensing, . 10.1109/TGRS.2008.2011892.

Published

2014-07-03